The Story of the HeavensBall, Robert S. (Robert Stawell)
History
The Story of the Heavens
Ball, Robert S. (Robert Stawell)
Astronomy
It is well to illustrate this remarkable law by considering the
circumstances of two or three different planets. Take first the case of
the earth, the path of which, though really an ellipse, is very nearly
circular. In fact, if it were drawn accurately to scale on a sheet of
paper, the difference between the elliptic orbit and the circle would
hardly be detected without careful measurement. In the case of Venus the
ellipse is still more nearly a circle, and the two foci of the ellipse
are very nearly coincident with the centre of the circle. On the other
hand, in the case of Mercury, we have an ellipse which departs from the
circle to a very marked extent, while in the orbits of some of the minor
planets the eccentricity is still greater. It is extremely remarkable
that every planet, no matter how far from the sun, should be found to
move in an ellipse of some shape or other. We shall presently show that
necessity compels each planet to pursue an elliptic path, and that no
other form of path is possible.
Started on its elliptic path, the planet pursues its stately course, and
after a certain duration, known as the _periodic time_, regains the
position from which its departure was taken. Again the planet traces out
anew the same elliptic path, and thus, revolution after revolution, an
identical track is traversed around the sun. Let us now attempt to
follow the body in its course, and observe the history of its motion
during the time requisite for the completion of one of its circuits. The
dimensions of a planetary orbit are so stupendous that the planet must
run its course very rapidly in order to finish the journey within the
allotted time. The earth, as we have already seen, has to move eighteen
miles a second to accomplish one of its voyages round the sun in the
lapse of 365-1/4 days. The question then arises as to whether the rate
at which a planet moves is uniform or not. Does the earth, for instance,
actually move at all times with the velocity of eighteen miles a
second, or does our planet sometimes move more rapidly and sometimes
more slowly, so that the average of eighteen miles a second is still
maintained? This is a question of very great importance, and we are able
to answer it in the clearest and most emphatic manner. The velocity of a
planet is _not_ uniform, and the variations of that velocity can be
explained by the adjoining figure (Fig. 38).
[Illustration: Fig. 38.--Varying Velocity of Elliptic Motion.]
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